Enceladus's and Dione's floating ice shells supported by minimum stress isostasy-Reference-Cited by-同舟云学术

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Enceladus's and Dione's floating ice shells supported by minimum stress isostasy

Published:2016-10-09 Issue:19 Volume:43 Page:10,088-10,096
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Beuthe Mikael¹,Rivoldini Attilio¹,Trinh Antony¹

Affiliation:

1. Royal Observatory of Belgium; Brussels Belgium

Funder

Brain Pioneer

Federaal Wetenschapsbeleid

European Research Council

European Union's Horizon 2020

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GL070650/fullpdf

Reference51 articles.

1. Convection-driven compaction as a possible origin of Enceladus's long wavelength topography;Besserer;J. Geophys. Res. Planets,2013

2. Enceladus's internal ocean and ice shell constrained from Cassini gravity, shape and libration data;Cadek, O.;Geophys. Res. Lett.,2016

3. Structural mapping of Enceladus and implications for formation of tectonized regions;Crow-Willard;J. Geophys. Res. Planets,2015

4. Isostasy and the ambient state of stress in the oceanic lithosphere;Dahlen;J. Geophys. Res.,1981

5. Isostatic geoid anomalies on a sphere;Dahlen;J. Geophys. Res.,1982

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